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| 1 | Subcritieal water extraction of trace metals from petroleum source rock 显示文摘 | AKINLUA A SMITH R M | 2010 | Talanta2010，81，45： | 1 |
| 2 | Trace element characterisation of Cretaceous Orange Basin hydrocar bon source rocks显示文摘 | Akinlua A Adekola S A Swakamisa O | | 0，，10： | 1 |
| 3 | Supercritical fluid ex- traction of aliphatic hydrocarbons from Niger Delta sedimen- tary rock显示文摘 | Akinlua A Torto N Ajayi T R | 2008 | Journal of Supercritical Fluids2008，45，1： | 1 |
| 4 | Determination ofrare earth elements in Niger Delta crude oils byinductively coupled plasma-mass spectrometry显示文摘 | Akinlua A Torto N Ajayi T R | 2008 | Fuel2008，87，8： | 1 |
| 5 | Organic and inorganic geochemistry of northwestern Niger Delta oils显示文摘 | Akinlua A Ajayi T R Adeleke B B | | 0，，04： | 1 |
| 6 | Provenance, diagene-sis and reservoir quality of the Lower Cretaceous sandstone ofthe Orange Basin, South Africa显示文摘 | Fadipe () A Carey P F Akinlua A | 2011 | South African Journal ofGeology2011，114，： | 1 |
| 7 | Niger Delta oil geochemis- try:Insight from light hydrocarbons显示文摘 | Akinlua A Ajayi T R Adeleke B B | 2006 | Journal of Petroleum Sci- ence and Engineering2006，50，34： | 1 |
| 8 | Determination of rare earth elements in Niger Delta crude oils by inductively coupled plasma-mass spectrometry 显示文摘 | Akinlua A Torto N Ajayi T R | 2008 | Science Direct Fuel2008，87，： | 1 |
| 9 | Provenance, Diagenesis and reservoir quality of the lower Cretaceous sandstone of the Orange Basin, South Africa显示文摘 | FADIPE O A CAREY P F AKINLUA A | 2011 | South African Journal of Geology2011，114，34： | 1 |
| 10 | Source rock geochemistry of central and northwestern Niger Delta: Inference from aromatic hydrocarbons content显示文摘The influence of origin, depositional environment and thermal maturity of organic matter on the occurrence of aromatic hydrocarbons in source rocks from the central and northwestern Niger Delta was investigated. Eighty two source rock samples from four oil wells in the central and northwestern Niger Delta were analyzed for the aromatic hydrocarbon content using gas chromatography-mass spectrometry (GC-MS). The results of analysis of aromatic hydrocarbon fractions of the source rock extracts show the presence of many classes of aromatic hydrocarbons, which include naphthalenes, phenanthrenes, biphenyls, dibenzothiophenes and fluorenes. Trimethylnaphthalene (TMN) is the most abundant among the naphthalenes while dimethylphenanthrene (DMP) is the most abundant among the phenanthrenes. Among the biphenyls, 3-methylbiphenyl (3 MB) is the most abundant while 4-methyldibenzothiophene (4MDBT) is the most abundant among the dibenzothiphenes. Only two fluorenes were detected, and fluorene is more in abundance than 1-methylfluorene (1 MF). Depositional environment indicators of aromatic hydrocarbon organic matter reveal that the organic materials in the source rocks in these wells were deposited in marine-to-swamp depositional environments under reducing to suboxic conditions. Thermal maturity indicators calculated from the abundance of the aromatic hydrocarbons indicate that the source rock samples are thermally mature. Most of the source rocks are at the peak of oil window while a few at the early oil window. Source rocks from wells GB, OP and OT in the central Niger Delta are thermally more mature than those from well AW in the northwestern Niger Delta. | Akinsehinwa Akinlua Olugbemiga Raphael Dada Fuad Oluseyi Usman Solomon Adeniyi Adekola | 2023 | Energy Geoscience2023，4，3： | 0 |
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